Sensitivity of the LMD General Circulation Model to Greenhouse Forcing Associated with Two Different Cloud Water Parameterizations

Abstract The atmospheric general circulation model of the Laboratoire de Meteorologic Dynamique is coupled to a slab ocean model and is used to investigate the climatic impact of a C02 doubling. Two versions of the model are used with two different representations of the cloud-radiation interaction. Both of them contain a prognostic equation for the cloud liquid water content, but they differ in the treatment of the precipitation mechanism. The annual and global mean of the surface warming is similar in the two experiments in spite of regional differences. To understand the behavior of the model versions, the total climate change is split into a direct C02 forcing and different feedback effects (water vapor. cloud, and surface albedo). The results show that, in the second model version, the cloud feedback decreases significantly, especially at high latitudes, due to an increase of low-level clouds in the 2×C02 simulation. The modification of the cloud scheme influences also the water vapor variation and t...

[1]  A. Oort,et al.  Global atmospheric circulation statistics, 1958-1973 , 1994 .

[2]  H. Treut,et al.  Solar dynamics and its impact on solar irradiance and the terrestrial climate , 1993 .

[3]  John F. B. Mitchell,et al.  Carbon Dioxide and Climate. The Impact of Cloud Parameterization , 1993 .

[4]  S. Bony,et al.  Satellite validation of GCM-simulated annual cycle of the Earth radiation budget and cloud forcing , 1992 .

[5]  Norman A. McFarlane,et al.  Greenhouse Gas–induced Climate Change Simulated with the CCC Second-Generation General Circulation Model , 1992 .

[6]  Hervé Le Treut,et al.  Cloud-radiation feedbacks in a general circulation model and their dependence on cloud modelling assumptions , 1992 .

[7]  K. Emanuel A Scheme for Representing Cumulus Convection in Large-Scale Models , 1991 .

[8]  Zhaoxin Li,et al.  Sensitivity of an atmospheric general circulation model to prescribed SST changes: feedback effects associated with the simulation of cloud optical properties , 1991 .

[9]  John F. B. Mitchell,et al.  Intercomparison and interpretation of climate feedback processes in 19 atmospheric general circulation models , 1990 .

[10]  Andrew J. Heymsfield,et al.  A scheme for parameterizing ice cloud water content in general circulation models , 1990 .

[11]  M. Herman,et al.  The influence of clouds on radiation: A climate‐modeling perspective , 1990 .

[12]  J. Mitchell,et al.  C02 and climate: a missing feedback? , 1989, Nature.

[13]  Michael E. Schlesinger,et al.  Seasonal Climatic Changes Induced by Doubled CO2 as Simulated by the OSU Atmospheric GCM/Mixed-Layer Ocean Model , 1989 .

[14]  B. Barkstrom,et al.  Cloud-Radiative Forcing and Climate: Results from the Earth Radiation Budget Experiment , 1989, Science.

[15]  Gerald L. Potter,et al.  A methodology for understanding and intercomparing atmospheric climate feedback processes in general circulation models , 1988 .

[16]  S. Manabe,et al.  Cloud Feedback Processes in a General Circulation Model , 1988 .

[17]  Cara Wilson,et al.  A doubled CO2 climate sensitivity experiment with a global climate model including a simple ocean , 1987 .

[18]  E. Roeckner,et al.  Cloud optical depth feedbacks and climate modelling , 1987, Nature.

[19]  Michael E. Schlesinger,et al.  Climate Model Simulations of the Equilibrium Climatic Response to Increased Carbon Dioxide (Paper 6R0726) , 1987 .

[20]  Stephen K. Cox,et al.  Cirrus Clouds. Part I: A Cirrus Cloud Model , 1985 .

[21]  G. Meehl,et al.  Seasonal cycle experiment on the climate sensitivity due to a doubling of CO2 with an atmospheric general circulation model coupled to a simple mixed‐layer ocean model , 1984 .

[22]  R. Somerville Cloud optical thickness feedbacks in the CO2 climate problem , 1984 .

[23]  Hilding Sundqvist,et al.  Prediction of stratiform clouds: Results from a 5-day forecast with a global model , 1981 .

[24]  Peter J. Webster,et al.  Clouds and Climate: Sensitivity of Simple Systems. , 1981 .

[25]  Syukuro Manabe,et al.  Sensitivity of a global climate model to an increase of CO2 concentration in the atmosphere , 1980 .

[26]  W. Ingram,et al.  Carbon Dioxide and Climate: Mechanisms of Changes in Cloud , 1992 .

[27]  R. Smith A scheme for predicting layer clouds and their water content in a general circulation model , 1990 .

[28]  B. J. Mason,et al.  The physics of clouds , 1971 .

[29]  E. Kessler On the distribution and continuity of water substance in atmospheric circulations , 1969 .

[30]  H. Kuo On Formation and Intensification of Tropical Cyclones Through Latent Heat Release by Cumulus Convection , 1965 .